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  • 1
    Online Resource
    Online Resource
    Journal of Marine Research/Yale ; 1991
    In:  Journal of Marine Research Vol. 49, No. 2 ( 1991-05-01), p. 281-294
    In: Journal of Marine Research, Journal of Marine Research/Yale, Vol. 49, No. 2 ( 1991-05-01), p. 281-294
    Type of Medium: Online Resource
    ISSN: 0022-2402 , 1543-9542
    Language: English
    Publisher: Journal of Marine Research/Yale
    Publication Date: 1991
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    SSG: 12
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    Elsevier BV ; 1986
    In:  Deep Sea Research Part A. Oceanographic Research Papers Vol. 33, No. 2 ( 1986-2), p. 209-223
    In: Deep Sea Research Part A. Oceanographic Research Papers, Elsevier BV, Vol. 33, No. 2 ( 1986-2), p. 209-223
    Type of Medium: Online Resource
    ISSN: 0198-0149
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1986
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    Location Call Number Limitation Availability
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1999
    In:  Journal of Geophysical Research: Oceans Vol. 104, No. C9 ( 1999-09-15), p. 20859-20861
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 104, No. C9 ( 1999-09-15), p. 20859-20861
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1999
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    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
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    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1998
    In:  Journal of Geophysical Research: Oceans Vol. 103, No. C8 ( 1998-07-15), p. 15869-15883
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 103, No. C8 ( 1998-07-15), p. 15869-15883
    Abstract: Four World Ocean Circulation Experiment (WOCE) repeat cruises (October 1990 to March 1994) in the tropical Atlantic off Brazil are used to study the spatial and temporal evolution of the chlorofluorocarbon (CFC) (components CFC‐11 and CFC‐12) and tritium signal in the upper North Atlantic Deep Water (NADW). Its shallowest part, located in the tropical Atlantic around 1600‐m depth, is the shallow upper North Atlantic Deep Water (SUNADW). It is characterized by a distinct tracer maximum, which is presumably received through winter time convection in the subpolar North Atlantic. Here we discuss the tracer fields and the temporal evolution of the tracer signal of the SUNADW in the tropical Atlantic along two meridional sections at 44° and 35°W and two zonal sections at 5° and 10°S off Brazil. The spatial and temporal development of the tracer field in the tropical Atlantic as well as the correlation with hydrographic parameters show that the temporal tracer change being due to the arrival of “younger” water is disturbed by other processes. In particular, the impact of variable mixing and spreading pathways on the observed tracer variability in the SUNADW is evident in the observations.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1998
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    detail.hit.zdb_id: 3094104-0
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    detail.hit.zdb_id: 2403298-0
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    detail.hit.zdb_id: 161667-5
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    detail.hit.zdb_id: 3094268-8
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  • 5
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1987
    In:  Journal of Geophysical Research: Oceans Vol. 92, No. C12 ( 1987-11-15), p. 12993-13002
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 92, No. C12 ( 1987-11-15), p. 12993-13002
    Abstract: Reducing the large volume of TIROS‐N series advanced very high resolution radiometer‐derived data to a practical size for application to regional physcial oceanographic studies is a formidable task. Such data exist on a global basis for January 1979 to the present at approximately 4‐km resolution (global area coverage data, ≈2 passes per day) and in selected areas at high resolution (local area coverage and high‐resolution picture transmission data, at ≈1‐km resolution) for the same period. An approach that has been successful for a number of studies off the east coast of the United States divided the processing into two procedures: preprocessing and data reduction. The preprocessing procedure can reduce the data volume per satellite pass by over 98% for full‐resolution data or by ≈84% for the lower‐resolution data while the number of passes remains unchanged. The output of the preprocessing procedure for the examples presented is a set of sea surface temperature (SST) fields of 512 × 1024 pixels covering a region of approximately 2000 × 4000 km. In the data reduction procedure the number of SST fields (beginning with one per satellite pass) is generally reduced to a number manageable from the analyst's perspective (of the order of one SST field per day). This is done in most of the applications presented by compositing the data into 1‐ or 2‐day groups. The phenomena readily addressed by such procedures are the mean position of the Gulf Stream, the envelope of Gulf Stream meandering, cold core Gulf Stream ring trajectories, statistics on diurnal warming, and the region and period of 18°C water formation. The flexibility of this approach to regional oceanographic problems will certainly extend the list of applications quickly.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1987
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    detail.hit.zdb_id: 2969341-X
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    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
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    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1988
    In:  Journal of Geophysical Research: Oceans Vol. 93, No. C7 ( 1988-07-15), p. 8111-8118
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 93, No. C7 ( 1988-07-15), p. 8111-8118
    Abstract: The eastern part of the North Atlantic subtropical gyre is found in the region between the Azores and the Cape Verde Islands. A study of the gyre structure in the area east of 35°W between 8°N and 41°N is presented. The geostrophic flow field determined from historical temperature‐salinity data sets by objective analysis indicates seasonal variations in shape but no significant changes in the magnitude of volume transports. The eastern part of the gyre has a larger east‐west and smaller north‐south extension in summer compared with the winter season. The center shifts by about 2° latitude to the south from winter to summer. Long‐term temperature time series (6.5 years) from a mooring near the Azores are consistent with these results, showing always a consistent temperature increase at the beginning of the year which is apparently due to the displacement of the northeastern part of the gyre. A comparison between the mean flow fields and fields obtained from individual zonal sections indicates large deviations north and south of the gyre but small deviations within the gyre.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1988
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    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
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    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2008
    In:  Geophysical Research Letters Vol. 35, No. 10 ( 2008-05)
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 35, No. 10 ( 2008-05)
    Abstract: A new version of SODA, which covers the time period 1958–2005, is used to analyze decadal variability of the Pacific Subtropical Cell (STC) circulation. The analysis is based on transport time series across 9°S and 9°N. At the interannual time scale, STC convergence anomalies decrease during El Niños and increase during La Niñas through Sverdrup transport convergence changes. At decadal time scales, the assimilation shows a reduction of interior STC convergence of about 8 Sv from the 1960s to the 1990s and a subsequent rebound into the early 2000s by a similar amount, in agreement with the STC tendencies reported earlier from geostrophic section analysis, and associated with the occurrence and intensity of ENSO events among the decades analyzed. The results are compared with, and differ significantly from, those obtained by the German ECCO (GECCO) assimilation.
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2008
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  • 8
    Online Resource
    Online Resource
    Elsevier BV ; 2002
    In:  Deep Sea Research Part II: Topical Studies in Oceanography Vol. 49, No. 7-8 ( 2002-1), p. 1197-1210
    In: Deep Sea Research Part II: Topical Studies in Oceanography, Elsevier BV, Vol. 49, No. 7-8 ( 2002-1), p. 1197-1210
    Type of Medium: Online Resource
    ISSN: 0967-0645
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2002
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    detail.hit.zdb_id: 1500312-7
    SSG: 14
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  • 9
    Online Resource
    Online Resource
    Elsevier BV ; 2002
    In:  Deep Sea Research Part II: Topical Studies in Oceanography Vol. 49, No. 7-8 ( 2002-1), p. 1173-1195
    In: Deep Sea Research Part II: Topical Studies in Oceanography, Elsevier BV, Vol. 49, No. 7-8 ( 2002-1), p. 1173-1195
    Type of Medium: Online Resource
    ISSN: 0967-0645
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2002
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    detail.hit.zdb_id: 1500312-7
    SSG: 14
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  • 10
    In: Geochimica et Cosmochimica Acta, Elsevier BV, Vol. 99 ( 2012-12), p. 128-145
    Type of Medium: Online Resource
    ISSN: 0016-7037
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2012
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    detail.hit.zdb_id: 1483679-8
    SSG: 13
    SSG: 16,12
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